AustralieFrV1, PascalFrancis, Curation, bibRecord, 001F60

Ellipsis 3D : A particle-in-cell finite-element hybrid code for modelling mantle convection and lithospheric deformation

Identifieur interne : 001F60 ( PascalFrancis/Curation ); précédent : 001F59; suivant : 001F61

Ellipsis 3D : A particle-in-cell finite-element hybrid code for modelling mantle convection and lithospheric deformation

Auteurs : Craig O'Neill [Australie] ; Louis Moresi [Australie] ; Dietmar Müller [Australie] ; Rich Albert [États-Unis] ; Frédéric Dufour [France]

Source :

Computers & geosciences [ 0098-3004 ] ; 2006.

RBID : Pascal:06-0461911

Descripteurs français

Pascal (Inist)
- Particule, Méthode élément fini, Modèle 3 dimensions, Manteau, Convection, Déformation sous contrainte, Géodynamique, Interface, Distorsion, Extension, Panache, Lithosphère, Ordinateur, Traitement donnée, Déformation, Modèle 2 couches.
Wicri :
- topic : Ordinateur.

English descriptors

KwdEn :
- computers, convection, data processing, deformation, distortion, extension, finite element analysis, geodynamics, interfaces, lithosphere, mantle, particles, plumes, strain, three-dimensional models, two-layer models.

Abstract

We have extended the two-dimensional geodynamics finite-element code "Ellipsis" to three-dimensions. Ellipsis uses a hybrid particle in a cell scheme, which combines a fixed mesh of computational points and a dense arrangement of mobile material points. The fixed Eulerian mesh allows very fast computation, performed in Ellipsis via a multigrid iteration method, while the Lagrangian particle reference frame allows the tracking of material interfaces and history-dependent properties such as strain history for strain-softening materials. The method is exceptionally useful in very large deformation analyses, where purely Lagrangian approaches would be severely hampered by the need for remeshing to minimize element distortion. The Gnu Public Licensed Ellipsis3D code lends itself to combined 2D/3D model prototyping, and has proven to be an excellent geodynamics teaching tool for modelling, covering mantle convection, lithospheric extension and plume-lithosphere interaction.

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A08	`01`	`1`	`ENG`	`@1 Ellipsis 3D : A particle-in-cell finite-element hybrid code for modelling mantle convection and lithospheric deformation`
A11	`01`	`1`		`@1 O'NEILL (Craig)`
A11	`02`	`1`		`@1 MORESI (Louis)`
A11	`03`	`1`		`@1 MÜLLER (Dietmar)`
A11	`04`	`1`		`@1 ALBERT (Rich)`
A11	`05`	`1`		`@1 DUFOUR (Frédéric)`
A14	`01`			`@1 School of Earth Sciences, The University of Sydney @2 Sydney, NSW, 2006 @3 AUS @Z 1 aut. @Z 3 aut.`
A14	`02`			`@1 School of Mathematical Sciences, Monash University @2 Victoria @3 AUS @Z 2 aut.`
A14	`03`			`@1 Exxon Mobil Exploration Co @2 Houston, TX @3 USA @Z 4 aut.`
A14	`04`			`@1 Ecole Centrale de Nantes @3 FRA @Z 5 aut.`
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C01	`01`		`ENG`	@0 We have extended the two-dimensional geodynamics finite-element code "Ellipsis" to three-dimensions. Ellipsis uses a hybrid particle in a cell scheme, which combines a fixed mesh of computational points and a dense arrangement of mobile material points. The fixed Eulerian mesh allows very fast computation, performed in Ellipsis via a multigrid iteration method, while the Lagrangian particle reference frame allows the tracking of material interfaces and history-dependent properties such as strain history for strain-softening materials. The method is exceptionally useful in very large deformation analyses, where purely Lagrangian approaches would be severely hampered by the need for remeshing to minimize element distortion. The Gnu Public Licensed Ellipsis3D code lends itself to combined 2D/3D model prototyping, and has proven to be an excellent geodynamics teaching tool for modelling, covering mantle convection, lithospheric extension and plume-lithosphere interaction.
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C03	`03`	`2`	`ENG`	`@0 three-dimensional models @5 03`
C03	`03`	`2`	`SPA`	`@0 Modelo 3 dimensiones @5 03`
C03	`04`	`2`	`FRE`	`@0 Manteau @5 04`
C03	`04`	`2`	`ENG`	`@0 mantle @5 04`
C03	`04`	`2`	`SPA`	`@0 Abrigo @5 04`
C03	`05`	`2`	`FRE`	`@0 Convection @5 05`
C03	`05`	`2`	`ENG`	`@0 convection @5 05`
C03	`05`	`2`	`SPA`	`@0 Convección @5 05`
C03	`06`	`2`	`FRE`	`@0 Déformation sous contrainte @5 06`
C03	`06`	`2`	`ENG`	`@0 strain @5 06`
C03	`06`	`2`	`SPA`	`@0 Deformación bajo tensión @5 06`
C03	`07`	`2`	`FRE`	`@0 Géodynamique @5 07`
C03	`07`	`2`	`ENG`	`@0 geodynamics @5 07`
C03	`07`	`2`	`SPA`	`@0 Geodinámica @5 07`
C03	`08`	`2`	`FRE`	`@0 Interface @5 09`
C03	`08`	`2`	`ENG`	`@0 interfaces @5 09`
C03	`08`	`2`	`SPA`	`@0 Interfase @5 09`
C03	`09`	`2`	`FRE`	`@0 Distorsion @5 10`
C03	`09`	`2`	`ENG`	`@0 distortion @5 10`
C03	`09`	`2`	`SPA`	`@0 Distorsión @5 10`
C03	`10`	`2`	`FRE`	`@0 Extension @5 11`
C03	`10`	`2`	`ENG`	`@0 extension @5 11`
C03	`10`	`2`	`SPA`	`@0 Extensión @5 11`
C03	`11`	`2`	`FRE`	`@0 Panache @5 12`
C03	`11`	`2`	`ENG`	`@0 plumes @5 12`
C03	`11`	`2`	`SPA`	`@0 Penacho @5 12`
C03	`12`	`2`	`FRE`	`@0 Lithosphère @5 13`
C03	`12`	`2`	`ENG`	`@0 lithosphere @5 13`
C03	`12`	`2`	`SPA`	`@0 Litosfera @5 13`
C03	`13`	`2`	`FRE`	`@0 Ordinateur @5 14`
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C03	`14`	`2`	`FRE`	`@0 Traitement donnée @5 15`
C03	`14`	`2`	`ENG`	`@0 data processing @5 15`
C03	`14`	`2`	`SPA`	`@0 Tratamiento datos @5 15`
C03	`15`	`2`	`FRE`	`@0 Déformation @5 16`
C03	`15`	`2`	`ENG`	`@0 deformation @5 16`
C03	`16`	`2`	`FRE`	`@0 Modèle 2 couches @5 17`
C03	`16`	`2`	`ENG`	`@0 two-layer models @5 17`
C03	`16`	`2`	`SPA`	`@0 Modelo 2 capas @5 17`
C06				`@0 ILS`
N21				`@1 303`

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Le document en format XML

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<front><div type="abstract" xml:lang="en">We have extended the two-dimensional geodynamics finite-element code "Ellipsis" to three-dimensions. Ellipsis uses a hybrid particle in a cell scheme, which combines a fixed mesh of computational points and a dense arrangement of mobile material points. The fixed Eulerian mesh allows very fast computation, performed in Ellipsis via a multigrid iteration method, while the Lagrangian particle reference frame allows the tracking of material interfaces and history-dependent properties such as strain history for strain-softening materials. The method is exceptionally useful in very large deformation analyses, where purely Lagrangian approaches would be severely hampered by the need for remeshing to minimize element distortion. The Gnu Public Licensed Ellipsis3D code lends itself to combined 2D/3D model prototyping, and has proven to be an excellent geodynamics teaching tool for modelling, covering mantle convection, lithospheric extension and plume-lithosphere interaction.</div>
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<fC01 i1="01" l="ENG"><s0>We have extended the two-dimensional geodynamics finite-element code "Ellipsis" to three-dimensions. Ellipsis uses a hybrid particle in a cell scheme, which combines a fixed mesh of computational points and a dense arrangement of mobile material points. The fixed Eulerian mesh allows very fast computation, performed in Ellipsis via a multigrid iteration method, while the Lagrangian particle reference frame allows the tracking of material interfaces and history-dependent properties such as strain history for strain-softening materials. The method is exceptionally useful in very large deformation analyses, where purely Lagrangian approaches would be severely hampered by the need for remeshing to minimize element distortion. The Gnu Public Licensed Ellipsis3D code lends itself to combined 2D/3D model prototyping, and has proven to be an excellent geodynamics teaching tool for modelling, covering mantle convection, lithospheric extension and plume-lithosphere interaction.</s0>
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<s5>04</s5>
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<s5>04</s5>
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<s5>05</s5>
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<s5>05</s5>
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<s5>05</s5>
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<s5>06</s5>
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<fC03 i1="06" i2="2" l="ENG"><s0>strain</s0>
<s5>06</s5>
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<s5>06</s5>
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<s5>07</s5>
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<s5>07</s5>
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<s5>09</s5>
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<s5>09</s5>
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<s5>09</s5>
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<fC03 i1="09" i2="2" l="FRE"><s0>Distorsion</s0>
<s5>10</s5>
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<fC03 i1="09" i2="2" l="ENG"><s0>distortion</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Distorsión</s0>
<s5>10</s5>
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<fC03 i1="10" i2="2" l="FRE"><s0>Extension</s0>
<s5>11</s5>
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<fC03 i1="10" i2="2" l="ENG"><s0>extension</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Extensión</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Panache</s0>
<s5>12</s5>
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<fC03 i1="11" i2="2" l="ENG"><s0>plumes</s0>
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	Serveur d'exploration sur les relations entre la France et l'Australie
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Ellipsis 3D : A particle-in-cell finite-element hybrid code for modelling mantle convection and lithospheric deformation

Ellipsis 3D : A particle-in-cell finite-element hybrid code for modelling mantle convection and lithospheric deformation

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